沙尔布尔铁矿床形成于古岛弧区内的局部拉张环境。
Shaerbuer Iron deposit was formed in a partial tension environment of an ancient arc zone.
河坎子碱性杂岩体形成于板内拉张环境，岩浆作用以批式部分熔融占主导地位。
Variation diagrams of major and trace elements imply that the Hekanzi alkaline complex was formed in an intra-plate environment, and its major magmatic process is dominated by batch melting.
说明了地幔隆起可在盆地区产生拉张环境，正是这种拉张应力场导致了地裂缝的产生。
The simulation results show that a tension stress field is produced with mantle lifting up.
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